A Memory of Ancient Ices Preserved in Carbonaceous Chondrite Matrices

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Scientific paper

Abundances of H2O, C and N in CC become zero when Delta
18O ~ 3?, corresponding to 30-40% matrix in the rock probably
as rims on chondrules. CC inherited a common component, ice with IOM
with C/N = 22, accreted only in their interstitial "true matrix."

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